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sinkhole noun [C] (HOLE) abyss (HOLE) literary. canyon. chasm. cleft. crater noun. crevasse. defile noun literary. gorge noun (VALLEY)
Sinkholes are all about water. Water dissolved minerals in the rock, leaving residue and open spaces within the rock. Water washes away the soil and residue from the voids in the rock. Lowering of groundwater levels can cause a loss of support for the soft material in the rock spaces that can lead to collapse.
The underground water of Karst topography carves our impressive channels and caves that are susceptible to collapse from the surface. When enough limestone is eroded from underground, a sinkhole (also called a doline) may develop. Sinkholes are depresstions that form when a portion the lithosphere below is eroded away.
Protecting natural water sources, such as rivers, lakes, and aquifers, is essential for sinkhole prevention. Unregulated extraction of groundwater can lead to subsidence and the formation of sinkholes.
Sinkholes are formed when the land surface above collapses or sinks into the cavities or when surface material is carried downward into the voids. Drought, along with resulting high groundwater withdrawals, can make conditions favorable for sinkholes to form.
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Sinkholes have been reported along seismically active faults indicating a causal link between sinkholes and tectonics. The processes responsible for their formation may be related to fracturing in the fault damage zone, promoting fluid circulation and weathering of soluble rocks at depth.
Sink-hole, Swallet, Swallow. A sinkhole is a closed depression in karst (a landscape resulting from the dissolution of soluble rock) by current or palaeo internal drainage, also known as a doline.
Sinkholes typically form when naturally acidic rainwater erodes underlying bedrock, creating damage beneath the surface. Their formation is most common in easily erodible karst terrains with carbonate rocks, like limestone or dolomite, or minerals known as evaporites, like salt and gypsum.

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